VANCOUVER, BC, Sept. 23,
2024 /CNW/ - Nevada King Gold Corp.
(TSXV: NKG) (OTC: NKGFF) ("Nevada
King" or the "Company") is pleased to announce
assay results from twenty reverse circulation ("RC") holes
and one core hole recently completed at its Atlanta Gold Mine
Project located 264km northeast of Las
Vegas, Nevada, in the prolific Battle Mountain Trend.
Today's holes are plotted in plan and along sections 22-10N(4),
22-11N(3), 22-12N, and 22-13N, (Figures 1-5).
Highlights:
Hole
No.
|
From
(m)
|
To
(m)
|
Interval
(m)
|
Au
(g/t)
|
Ag
(g/t)
|
Section
|
AT23NS-120C+
|
15.4
|
69.2
|
53.8
|
4.10
|
32.9
|
10N(4)
|
Including
|
60.1
|
63.1
|
3.0
|
17.98
|
63.0
|
10N(4)
|
AT23NS-164
|
149.4
|
190.5
|
41.2
|
2.25
|
100.3
|
10N(4)
|
AT23NS-165
|
155.5
|
205.8
|
50.3
|
1.29
|
108.5
|
10N(4)
|
AT23NS-171*
|
118.9
|
154.0
|
35.1
|
3.59
|
37.1
|
12N
|
Including
|
138.7
|
141.8
|
3.0
|
18.88
|
48.2
|
12N
|
AT23NS-172
|
123.5
|
147.9
|
24.4
|
1.76
|
440.6
|
12N
|
Table 1.
Highlighted holes released today. True thickness of mineralization
along the steeply dipping West Atlanta Fault in holes NS-164 and
NS-165 is estimated to be 35% to 65% of reported drill intercept
length, while true thickness in the other holes is estimated to be
85% to 95% of reported intercept length. *Denotes holes bottoming in
mineralization. +Denotes core
holes.
|
- Shallow high-grade mineralization (4.10 g/t Au over
53.8m) in core hole
AT23NS-120C begins just 15.4m beneath the pit floor along the eastern
boundary of the Atlanta Mine Fault Zone ("AMFZ") and is
being used for ongoing Phase II metallurgical test work (Figure
2).
- AT23NS-171 and AT23NS-172 (Figures 3 and 4) were sited to fill
in drill gaps along the AMFZ and intersected 3.59 g/t Au
over 35.1m and 1.76 g/t Au
over 24.4m, respectively. Strong
silver values of 440.6 g/t Ag accompany the gold intercept
in AT23NS-172. These holes confirm that mineralization is
relatively flat-lying across the central portion of the AMFZ, with
higher-grade mineralization hosted in silicified rhyolitic
intrusions that moved laterally eastward from the West Atlanta
Fault ("WAF") along a gently west-dipping erosional
unconformity.
- AT23NS-164 (2.25 g/t Au over 41.2m) and AT23NS-165 (1.29 g/t Au over
50.3m) were positioned across a
drill gap on the eastern edge of the West Atlanta Graben Zone
("WAGZ") just west of the WAF. Mineralization is largely
hosted within silicified rhyolitic intrusive rock occurring along
the hanging wall side of the steeply-dipping WAF, although strongly
silicified Paleozoic basement rock beneath the silicified intrusive
hosts mineralization as well.
- Both types of strong silicification had previously been
lumped into the silica breccia unit, but the Company's relogging
campaign at Atlanta has now shown
most of the silica breccia unit to consist of rhyolitic intrusive
breccia based on trace element enrichment in chromium coupled with
depletion of titanium and magnesium. This is important because
these intrusions appear to have played a major role in decalcifying
carbonate host rocks and subsequently depositing Au/Ag throughout
the Atlanta deposit, which has
significant implications as the Company looks for new mineralized
zones within the carbonate-dominated regional targets recently
identified north and east of the resource zone (released
September 17, 2024).
Cal Herron, Exploration Manager
of Nevada King, stated, "Drilling
completed in and around the Atlanta resource zone continues to inform our
understanding behind the genesis of gold deposition at Atlanta. Throughout the West Atlanta Graben
Zone and up on the East Ridge Target, we know that rhyolitic
intrusions related to gold mineralization show up in the CSAMT data
as low resistivity zones. The Company has identified numerous
additional CSAMT low resistivity zones scattered throughout the
Atlanta district where other such
intrusive activity may have occurred.
"Based on our ongoing relogging program, we now recognize that
there are two distinct types of intrusive or silica breccia units
("SBX") found at Atlanta –
one associated with altered dolomite that rarely hosts gold
mineralization outside of the resource zone and the second related
to rhyolitic intrusions, which does often host gold mineralization.
As the regional drilling begins, this distinction between these two
SBX units will play an important role. SBX found to be high in
chromium and low in titanium/magnesium will indicate that we are
near to a rhyolitic event and with more searching, can reasonably
expect to find gold mineralization. On the other hand, SBX
encountered with elevated magnesium and low chromium values can be
quickly tagged as altered dolomite and disregarded if no anomalous
gold is present. Armed with this new exploration model, we feel
added confidence in our regional exploration program as we rely on
CSAMT signatures, looking for additional (and in many cases larger)
intrusive-related mineralized zones."
Hole
No.
|
From
(m)
|
To
(m)
|
Interval
(m)
|
Au
(g/t)
|
Ag
(g/t)
|
Section
|
AT23NS-120C+
|
15.4
|
6932
|
53.8
|
4.10
|
32.9
|
10N(4)
|
Including
|
60.1
|
63.1
|
3.0
|
17.98
|
63.0
|
10N(4)
|
AT23NS-164
|
149.4
|
190.5
|
41.2
|
2.25
|
100.3
|
10N(4)
|
AT23NS-165
|
155.5
|
205.8
|
50.3
|
1.29
|
108.5
|
10N(4)
|
AT23WS-65
|
355.2
|
382.6
|
27.4
|
1.09
|
16.3
|
11N(3)
|
AT23NS-172
|
123.5
|
147.9
|
24.4
|
1.76
|
440.6
|
11N(3)
|
AT24WS-66*
|
336.9
|
367.4
|
30.5
|
1.05
|
17.2
|
12N
|
AT22NS-86
|
61.0
|
88.4
|
27.4
|
1.10
|
22.1
|
12N
|
AT23NS-118
|
265.2
|
311.0
|
45.7
|
0.71
|
9.4
|
12N
|
AT23NS-169
|
178.4
|
202.7
|
24.4
|
2.45
|
55.5
|
12N
|
AT23NS-170
|
91.5
|
157.0
|
65.5
|
1.52
|
44.4
|
12N
|
AT23NS-171*
|
118.9
|
154.0
|
35.1
|
3.59
|
37.1
|
12N
|
Including
|
138.7
|
141.8
|
3.0
|
18.88
|
48.2
|
12N
|
AT21-18B^
|
0.0
|
4.6
|
6.7
|
0.15
|
22.97
|
13N
|
AT22NS-32
|
112.8
|
122.0
|
9.1
|
0.23
|
8.7
|
13N
|
AT22NS-33
|
35.1
|
45.7
|
10.7
|
0.47
|
118.2
|
13N
|
AT22NS-34
|
86.9
|
132.6
|
45.7
|
0.49
|
41.2
|
13N
|
AT22NS-35
|
27.4
|
36.6
|
9.1
|
0.44
|
44.9
|
13N
|
AT23WS-37
|
336.9
|
368.9
|
32.0
|
1.02
|
9.2
|
13N
|
AT22NS-93
|
176.8
|
201.2
|
24.4
|
1.53
|
24.9
|
13N
|
AT23NS-126
|
161.6
|
199.7
|
38.1
|
0.76
|
20.4
|
13N
|
AT23NS-132
|
189.0
|
236.3
|
47.3
|
1.25
|
30.3
|
13N
|
Table
2. All holes released today. Mineralization along the
northerly-trending West Atlanta Fault occurs within an intrusive
breccia zone dipping 60 to 70 west, and true mineralized thickness
is estimated to be 35% to 65% of reported intercept lengths. Holes
along the northerly-trending AMFZ and within the West Atlanta
Graben occur within gently dipping silica breccia above the
Paleozoic unconformity with true mineralized thickness of 85% to
95% of reported intercept lengths. * Denotes holes bottoming in
mineralization. ^
Denotes angle holes. +
Denotes core holes.
|
Hole
No.
|
From
(m)
|
To
(m)
|
Interval
(m)
|
Au
(g/t)
|
Ag
(g/t)
|
Section
|
AT22HG-18
|
257.6
|
291.2
|
33.5
|
2.35
|
363.0
|
10N(4)
|
AT23HG-26*
|
279.0
|
317.1
|
38.1
|
0.82
|
27.0
|
10N(4)
|
AT23WS-27
|
193.6
|
256.1
|
62.5
|
1.78
|
3.7
|
10N(4)
|
AT22NS-43A
|
3.0
|
30.5
|
27.4
|
1.02
|
21.2
|
10N(4)
|
AT22NS-46
|
4.6
|
59.5
|
54.9
|
3.41
|
26.0
|
10N(4)
|
AT22NS-47
|
64.0
|
89.9
|
25.9
|
2.04
|
27.8
|
10N(4)
|
AT23NS-48
|
91.5
|
112.8
|
21.3
|
1.27
|
35.1
|
10N(4)
|
AT22NS-49
|
62.5
|
88.4
|
25.9
|
3.73
|
46.1
|
10N(4)
|
Including
|
67.1
|
74.7
|
7.6
|
6.33
|
28.8
|
10N(4)
|
AT22NS-50
|
89.9
|
108.2
|
18.3
|
3.68
|
27.1
|
10N(4)
|
Including
|
93.0
|
99.1
|
6.1
|
7.09
|
33.1
|
10N(4)
|
AT22NS-89*
|
172.3
|
213.4
|
41.2
|
0.4
|
67.8
|
10N(4)
|
AT22NS-90
|
182.9
|
222.6
|
39.7
|
0.82
|
52.3
|
10N(4)
|
AT23NS-96
|
105.2
|
135.7
|
30.5
|
0.94
|
51.0
|
10N(4)
|
AT23NS-120
|
33.5
|
71.6
|
38.1
|
1.14
|
43.4
|
10N(4)
|
AT23NS-124
|
12.2
|
86.9
|
74.7
|
2.37
|
43.9
|
10N(4)
|
AT23NS-129
|
109.8
|
143.3
|
33.5
|
1.14
|
31.4
|
10N(4)
|
90-2
|
135.7
|
173.8
|
38.1
|
0.99
|
90.4
|
10N(4)
|
AR-02
|
182.9
|
205.7
|
22.8
|
1.72
|
46.9
|
10N(4)
|
AR-24
|
36.6
|
38.1
|
1.5
|
0.13
|
5.48
|
10N(4)
|
AT23WS-24
|
324.7
|
376.5
|
51.8
|
1.79
|
21.1
|
11N(3)
|
AT23WS-26
|
306.4
|
336.9
|
30.5
|
0.33
|
3.2
|
11N(3)
|
AT23WS-38
|
327.7
|
378.0
|
50.3
|
0.97
|
5.2
|
11N(3)
|
AT22NS-40
|
15.2
|
79.3
|
64.0
|
1.45
|
32.7
|
11N(3)
|
AT22NS-42
|
61.0
|
80.8
|
19.8
|
1.82
|
31.0
|
11N(3)
|
AT23NS-44
|
100.6
|
123.5
|
22.9
|
2.39
|
48.0
|
11N(3)
|
AT22NS-45
|
70.1
|
106.7
|
36.6
|
1.35
|
35.0
|
11N(3)
|
AT21-61
|
3.0
|
36.6
|
33.6
|
0.60
|
16.7
|
11N(3)
|
AT22NS-92
|
181.4
|
231.7
|
50.3
|
1.07
|
64.0
|
11N(3)
|
AT22NS-95
|
129.6
|
155.5
|
25.9
|
1.63
|
67.3
|
11N(3)
|
AT23NS-106
|
268.3
|
309.5
|
41.2
|
0.84
|
14.1
|
11N(3)
|
AT23NS-107
|
266.8
|
306.4
|
39.6
|
1.15
|
16.4
|
11N(3)
|
AT23NS-122
|
19.8
|
77.7
|
57.9
|
1.43
|
24.0
|
11N(3)
|
AT23NS-128
|
79.3
|
125.0
|
45.7
|
1.12
|
58.8
|
11N(3)
|
AT23NS-166
|
158.5
|
182.9
|
24.4
|
1.93
|
51.3
|
11N(3)
|
DHRI-11-NRC05
|
312.5
|
373.5
|
61.0
|
1.61
|
9.09
|
11N(3)
|
88-10
|
70.1
|
118.9
|
48.8
|
0.37
|
18.0
|
12N
|
KR98-19
|
192.0
|
216.4
|
24.4
|
1.23
|
44.63
|
12N
|
KR98-20
|
144.8
|
204.3
|
59.5
|
0.58
|
8.92
|
12N
|
DHRI-11-19C+
|
432.8
|
434.3
|
1.5
|
1.09
|
0.10
|
12N
|
DHRI-11-NRC06
|
300.2
|
355.1
|
54.9
|
0.49
|
11.5
|
12N
|
DHRI-15-LRC03*
|
289.5
|
338.3
|
48.8
|
1.26
|
5.31
|
12N
|
DHRI-15-LRC05
|
312.4
|
338.3
|
25.9
|
1.0
|
2.47
|
12N
|
DHRI-15-LRC06
|
303.3
|
341.4
|
38.1
|
0.51
|
1.96
|
12N
|
AT22RC-15
|
54.9
|
97.6
|
42.7
|
0.25
|
20.7
|
13N
|
AT21-18A
|
4.6
|
50.3
|
45.7
|
0.89
|
65.76
|
13N
|
AT21-19
|
16.8
|
29.0
|
12.2
|
0.11
|
<0.5
|
13N
|
AT21-20
|
19.8
|
27.4
|
7.6
|
<0.5
|
<0.5
|
13N
|
DHRI-11-02C^+
|
86.9
|
105.1
|
18.2
|
0.45
|
85.01
|
13N
|
DHRI-11-21C*
|
326.1
|
362.1
|
30.0
|
0.42
|
8.82
|
13N
|
DHRI-15-LRC04
|
297.2
|
339.9
|
42.7
|
0.74
|
2.07
|
13N
|
Table
3. Previously released holes drilled by Nevada
King and historic operators. Mineralization along the West Atlanta
Fault is estimated to be 35% to 65% of reported intercept lengths,
while true thickness in holes along the AMFZ and within the West
Atlanta Graben are estimated to be of 85% to 95% of reported
intercept lengths. AT series holes drilled by Nevada King in
2021 to 2023. DHRI series holes drilled by Meadow Bay in 2011 and
2015. 90 series holes drilled by Goldfields in 1990. 88 series
holes drilled by Bobcat in 1988. *Denotes holes bottoming in
mineralization. ^ Denotes angle drill holes. + Denotes core
holes.
|
QAQC Protocols
All RC samples from the Atlanta Project are split at the drill
site and placed in cloth and plastic bags utilizing a nominal 2kg
sample weight. CRF standards, blanks, and duplicates are inserted
into the sample stream on-site on a one-in-twenty sample basis,
meaning all three inserts are included in each 20-sample group.
Samples are shipped by a local contractor in large sample shipping
crates directly to American Assay Lab in Reno, Nevada, with full custody being
maintained at all times. At American Assay Lab, samples were
weighed then crushed to 75% passing 2mm and pulverized to 85%
passing 75 microns in order to produce a 300g pulverized split.
Prepared samples are initially run using a four acid + boric acid
digestion process and conventional multi-element ICP-OES analysis.
Gold assays are initially run using 30-gram samples by lead fire
assay with an OES finish to a 0.003 ppm detection limit, with
samples greater than 10 ppm finished gravimetrically. Silver
samples that run greater than 100ppm are also finished
gravimetrically. Every sample is also run through a cyanide leach
for gold with an ICP-OES finish. The QA/QC procedure involves
regular submission of Certified Analytical Standards and
property-specific duplicates.
Qualified Person
The scientific and technical information in this news release
has been reviewed and approved by Calvin R.
Herron, P.Geo., who is a Qualified Person as defined by
National Instrument 43-101 ("NI 43-101").
About Nevada King Gold Corp.
The Atlanta Mine is a historical gold-silver producer with a NI
43-101 compliant pit-constrained resource of 460,000 oz Au in the
measured and indicated category (11.0M tonnes at 1.3 g/t) plus an inferred
resource of 142,000 oz Au (5.3M
tonnes at 0.83 g/t). See the NI 43-101 Technical Report on
Resources titled "Atlanta Property, Lincoln County, NV" with an effective date of
October 6, 2020, and a report date of
December 22, 2020, as prepared by
Gustavson Associates and filed under the Company's profile on
SEDAR+ (www.sedarplus.ca).
Resource
Category
|
Tonnes
(000s)
|
Au
Grade
(ppm)
|
Contained Au
Oz
|
Ag
Grade
(ppm)
|
Contained Ag
Oz
|
Measured
|
4,130
|
1.51
|
200,000
|
14.0
|
1,860,000
|
Indicated
|
6,910
|
1.17
|
260,000
|
10.6
|
2,360,000
|
Measured +
Indicated
|
11,000
|
1.30
|
460,000
|
11.9
|
4,220,000
|
Inferred
|
5,310
|
0.83
|
142,000
|
7.3
|
1,240,000
|
Table 4. NI
43-101 Mineral Resources at the Atlanta Mine
|
Please see the Company's website at www.nevadaking.ca.
Neither the TSX Venture Exchange nor its Regulation Services
Provider (as that term is defined in the policies of the TSX
Venture Exchange) accepts responsibility for the adequacy or
accuracy of this release.
Cautionary Statements Regarding Forward Looking
Information
This news release contains certain "forward-looking
information" and "forward-looking statements" (collectively
"forward-looking statements") within the meaning of applicable
securities legislation. All statements, other than statements of
historical fact, included herein, without limitation, statements
relating the future operations and activities of Nevada King, are forward-looking statements.
Forward-looking statements are frequently, but not always,
identified by words such as "expects", "anticipates", "believes",
"intends", "estimates", "potential", "possible", and similar
expressions, or statements that events, conditions, or results
"will", "may", "could", or "should" occur or be achieved.
Forward-looking statements in this news release relate to, among
other things, the Company's exploration plans and the Company's
ability to potentially expand mineral resources and the impact
thereon. There can be no assurance that such statements will prove
to be accurate, and actual results and future events could differ
materially from those anticipated in such statements.
Forward-looking statements reflect the beliefs, opinions and
projections on the date the statements are made and are based upon
a number of assumptions and estimates that, while considered
reasonable by Nevada King, are
inherently subject to significant business, economic, competitive,
political and social uncertainties and contingencies. Many factors,
both known and unknown, could cause actual results, performance or
achievements to be materially different from the results,
performance or achievements that are or may be expressed or implied
by such forward-looking statements and the parties have made
assumptions and estimates based on or related to many of these
factors. Such factors include, without limitation, the ability to
complete proposed exploration work, the results of exploration,
continued availability of capital, and changes in general economic,
market and business conditions. Readers should not place undue
reliance on the forward-looking statements and information
contained in this news release concerning these items. Nevada King does not assume any obligation to
update the forward-looking statements of beliefs, opinions,
projections, or other factors, should they change, except as
required by applicable securities laws.
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SOURCE Nevada King Gold Corp.